{"title":"捷克共和国Barrandian地区konkonuprusy附近Jirásek采石场的中泥盆世(Eifelian, australian -ensensis带)牙形刺,特别强调Polygnathus pseudofoliatus群,并记录了Kačák期的环境变化","authors":"S. Vodrážková, T. Suttner","doi":"10.3140/bull.geosci.1774","DOIUrl":null,"url":null,"abstract":"conodont faunas, with particular emphasis on the Polygnathus pseudofoliatus Group. The material comes from the Jirásek quarry at Koněprusy (Fig. 1), which represents a unique section in the Barrandian area where the kockelianus–ensensis boundary interval corresponding to the Kačák Episode, is developed in a carbonate suc cession. (Note: In this paper we use the designation Kačák Episode sensu Walliser & Bultynck 2011, which better reflects its polyphase nature). Conodonts from the Jirásek quarry were previously studied by Kalvoda & Zikmundová in Galle & Hladil (1991), Kalvoda (1992) and Kalvoda in Hladil & Kalvoda (1993a, b). The following conodonts were reported by the above mentioned authors from the","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":"1 1","pages":"81-125"},"PeriodicalIF":1.5000,"publicationDate":"2020-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Middle Devonian (Eifelian, australis-ensensis zones) conodonts from the Jirásek quarry near Koněprusy (Barrandian area, Czech Republic) with special emphasis on the Polygnathus pseudofoliatus Group and notes on environmental changes related to the Kačák Episode\",\"authors\":\"S. Vodrážková, T. Suttner\",\"doi\":\"10.3140/bull.geosci.1774\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"conodont faunas, with particular emphasis on the Polygnathus pseudofoliatus Group. The material comes from the Jirásek quarry at Koněprusy (Fig. 1), which represents a unique section in the Barrandian area where the kockelianus–ensensis boundary interval corresponding to the Kačák Episode, is developed in a carbonate suc cession. (Note: In this paper we use the designation Kačák Episode sensu Walliser & Bultynck 2011, which better reflects its polyphase nature). Conodonts from the Jirásek quarry were previously studied by Kalvoda & Zikmundová in Galle & Hladil (1991), Kalvoda (1992) and Kalvoda in Hladil & Kalvoda (1993a, b). The following conodonts were reported by the above mentioned authors from the\",\"PeriodicalId\":9332,\"journal\":{\"name\":\"Bulletin of Geosciences\",\"volume\":\"1 1\",\"pages\":\"81-125\"},\"PeriodicalIF\":1.5000,\"publicationDate\":\"2020-03-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Bulletin of Geosciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.3140/bull.geosci.1774\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Geosciences","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.3140/bull.geosci.1774","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 3
摘要
牙形石动物群,特别强调假叶多颚群。该材料来自KonŞprussy的Jirásek采石场(图1),该采石场代表了Barrandian地区的一个独特地段,在该地段,与Kačák事件相对应的kockelianus–ensensis边界层段在碳酸盐岩沉积中发育。(注:在本文中,我们使用了Kačák Episop senso Walliser&Bultynck 2011的名称,这更好地反映了其多相性)。Kalvoda和Zikmundová在Galle和Hladil(1991年)、Kalvoda(1992年)和Kalvoda在Hladil和Kalvo达(1993年a,b)对Jirásek采石场的牙形刺进行了研究。上述作者从
Middle Devonian (Eifelian, australis-ensensis zones) conodonts from the Jirásek quarry near Koněprusy (Barrandian area, Czech Republic) with special emphasis on the Polygnathus pseudofoliatus Group and notes on environmental changes related to the Kačák Episode
conodont faunas, with particular emphasis on the Polygnathus pseudofoliatus Group. The material comes from the Jirásek quarry at Koněprusy (Fig. 1), which represents a unique section in the Barrandian area where the kockelianus–ensensis boundary interval corresponding to the Kačák Episode, is developed in a carbonate suc cession. (Note: In this paper we use the designation Kačák Episode sensu Walliser & Bultynck 2011, which better reflects its polyphase nature). Conodonts from the Jirásek quarry were previously studied by Kalvoda & Zikmundová in Galle & Hladil (1991), Kalvoda (1992) and Kalvoda in Hladil & Kalvoda (1993a, b). The following conodonts were reported by the above mentioned authors from the
期刊介绍:
The Bulletin of Geosciences is an international journal publishing original research papers, review articles, and short contributions concerning palaeoenvironmental geology, including palaeontology, stratigraphy, sedimentology, palaeogeography, palaeoecology, palaeoclimatology, geochemistry, mineralogy, geophysics, and related fields. All papers are subject to international peer review, and acceptance is based on quality alone.